| dc.contributor.author | Poulovassilis, A | en |
| dc.contributor.author | Kerkides, P | en |
| dc.contributor.author | Elmaloglou, S | en |
| dc.contributor.author | Argyrokastritis, I | en |
| dc.date.accessioned | 2014-06-06T06:42:01Z | |
| dc.date.available | 2014-06-06T06:42:01Z | |
| dc.date.issued | 1991 | en |
| dc.identifier.uri | http://dx.doi.org/10.1029/91WR00160 | en |
| dc.identifier.uri | http://62.217.125.90/xmlui/handle/123456789/383 | |
| dc.subject | Hydraulic Conductance | en |
| dc.subject | Infiltration Rate | en |
| dc.subject | Time Lag | en |
| dc.title | An investigation of the relationship between ponded and constant flux rainfall infiltration | en |
| heal.type | journalArticle | en |
| heal.identifier.primary | 10.1029/91WR00160 | en |
| heal.publicationDate | 1991 | en |
| heal.abstract | The physics of the rainfall infiltration under a constant rainfall flux greater than the hydraulic conductivity at saturation are investigated and compared with those pertaining to the infiltration process under flooding. From the arguments developed theoretically the following conclusions are reached: The moisture profile prevailing at the time the soil surface becomes saturated during the rainfall process (t = T) | en |
| heal.journalName | Water Resources Research | en |
| dc.identifier.doi | 10.1029/91WR00160 | en |
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